Category Archives: Geology

Fun Fact Friday January 27, 2023

It’s #funfactFriday folks! And today’s edition of the National Parks Traveler features a contribution from the Caldera Chronicles, a weekly feature produced by collaboration by scientists and the Yellowstone Volcano Observatory.

Today’s article is all about how the Grand Canyon of the Yellowstone came into being. Granted, it’s not like the Grand Canyon of Arizona, but it’s a pretty cool (and colorful) place all on it’s own, “Stretching from the Lower Falls to the Tower Falls area, the Grand Canyon of the Yellowstone is about 28 km (17 miles) long, 250–350 meters (820–1150 feet) deep, and 450–1200 meters (1500–4000 feet) across. It appears to be a surprisingly young feature of the region, having mostly formed during and immediately following the last ice age, within the past 20,000 years or so. “

To read more about this and view the video, click the image above.

These shots were captured during my autumn 2019 visit to Yellowstone National Park. I’d wanted to see the Lower Falls area back during the summer of 2018, as I made my way from TX to WA, but the crowds were horrendous and there was absolutely no place to park – seriously, every single parking space was filled. On the other hand, this visit resulting in these images was great – definitely no crowds.

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Fun Fact Friday, Geology, National Parks, Photography, Yellowstone National Park

Trivia Tuesday 11-15-2022

It’s Trivia Tuesday folks!

Morning Glory Pool in the Upper Geyser Basin of Yellowstone National Park is indeed a glory to behold, no matter what the season. But, if you’ve seen (and photographed) this hot spring in different seasons, under different lighting conditions, you’ll notice that the colors don’t look quite the same – in the cooler months, they tend to be a little less bright and a little more murky.

When this pool was first discovered it was a brilliant blue, hence the name after a beautiful morning glory flower. People throwing trash, coins, rocks and logs into this pool over the years have caused a change in the water temperature (cooling it because all that trash has piled up around the vent and reduced hot water circulation) which in turn has caused the colors to change, allowing orange- and yellow-colored bacteria to thrive within the water. Add to that the subfreezing temps of the winter season (when this photo was captured), which in turn cool the surface water of the hot spring, and you get a murky look like you see here. It’s still a beautiful little spring, but the change in colors is mainly due to the extreme short-sightednes of humans. Sigh.

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Geology, National Parks, Trivia Tuesday, Yellowstone National Park

Photography In The National Parks: An Exploration Of The Ice Age Floods National Geologic Trail – Part 2

A view of Echo Basin from the South Alcove of Frenchman Coulee, Channeled Scablands, Eastern Washington

September is a two-for-one month regarding photo columns published in the National Parks Traveler. The first article was about smartphone photography. This article is about a photographic visit to Frenchman Coulee in Eastern Washington, a feature of the Channeled Scablands along the Ice Age Floods National Geologic Trail.

To read this article, click on the image above.

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Filed under Channeled Scablands, Geology, Ice Age Floods National Geologic Trail, Photography, Photography In The National Parks

Fun Fact Friday, August 5, 2022: Exfoliation

It’s #FunFactFriday

Ok, be honest. What comes to mind when I write the word “exfoliation?” To me, a picture of dry, flaky skin first comes to mind. However, exfoliation has a geological context to it, too. It’s a weathering process and one of the best places to see this process is along Tioga Road in Yosemite National Park.

As you drive that road, take a look at the granite hills and domes all around you. Notice that interesting sort of “onion peel” effect on the rock layers? That’s exfoliation! It’s a type of weathering and is common in granites.

You see, granite formed beneath the earth’s surface, under immense pressure. So, when the surface sediments and rocks – collectively termed as overburden – covering that granite are eroded or removed and that granite is exposed, the pressure beneath which the granite lay is gone and the granite begins to expand, forming all sorts of fractures (joints). Weathering (like frost heaving) causes plates, or flakes of rock to strip away the surface rock much like onion skin peels away from the onion.

And now you know.

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Fun Fact Friday, Geology, National Parks, Photography, Yosemite National Park

One Heck Of A Pothole!

It’s Trivia Tuesday! So, what are you looking at in this image, you may be asking yourself. You see a teeny white SUV to the upper left of this image, some golden grass and scrubby sagebrush. You see a large hole in the center and center-left of the image. Well, that’s a pothole you are looking at. Yes, a pothole – like the ones your vehicle drives over and it doesn’t get fixed until some member of the city council or their relative damages their car driving over it and they demand it gets fixed. Only this pothole was created by something entirely different, and is out in the middle of Drumheller Channels National Natural Landmark, a part of the Channeled Scablands landscape seen along the Ice Age Floods National Geologic Trail in Eastern Washington state.

Ever heard of a “kolk”? Tens of thousands of years ago, colossal floodwaters surged through the area, higher than that white SUV, higher than any of the buttes you see in the image. Those waters were so strong and fast that they created corkscrew vortices called kolks (whirlpools) within the water. Those kolks drilled down into the ground and eroded and carried away boulders and soils to other destinations, leaving scraped and scoured landscape with these large potholes. And they are large. If you were to hike within the landscape of Drumheller Channels (much of which is located within the Columbia National Wildlife Refuge), you’d see dry potholes and water-filled potholes.

I’m writing a series of photo columns about the Channeled Scablands for the National Parks Traveler. Part 1 has already been published. Parts 2 and 3 are going to be published in later months.

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Channeled Scablands, Drumheller Channels National Natural Landmark, Eastern Washington, Geology, Ice Age Floods National Geologic Trail, National Parks, Travel, Trivia Tuesday, Washington State

Photography In The National Parks: Exploration Along The Ice Age Floods National Geologic Trail

Dry Falls Vista

The National Parks Traveler has published my latest photo column. This month, it’s all about my day trip to Eastern Washington’s Dry Falls and Channeled Scablands landscape along the Ice Age Floods National Geologic Trail.

To read the article, click on the image above.

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Eastern Washington, Geology, Ice Age Floods National Geologic Trail, National Parks Traveler, Photography, Travel, Washington State

Science In Yellowstone National Park

Colloidal Pool in Porcelain Basin was one of the hydrothermal features studied in the YVO 2021 annual report, Yellowstone National Park / photo by Rebecca Latson

Photography articles are not the only things about which I write for the National Parks Traveler. I also pen quizzes, park checklists, and itineraries, to name a few other pieces I contribute. Last week, you might have read a piece I wrote synopsizing a technical article about how scientists are running simulation scenarios for lahars (volcanic mudflows) that might occur due to an avalanche on Mount Rainier.

Today, the National Parks Traveler has published another article I’ve written: a synopsis of the 2021 annual report produced by the Yellowstone Volcano Observatory (YVO) of scientific research conducted over 2021 in Yellowstone National Park and some conclusions reached. It was a cool annual report to read and fun to condense into an article for the Traveler.

If you are interested in finding out what went on in Yellowstone National Park in 2021, and want to download the full 2021 YVO annual report, click on the image above.

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Filed under Geology, National Parks, National Parks Traveler, Yellowstone National Park

Lahars (Mudflows) Can’t Be Predicted, But They Can Be Simulated

A View Of Mount Rainier From Seattle’s Elliott Bay

Lahars (mudflows) can’t be predicted but they can be simulated using a special computer application. My latest contribution to the National Parks Traveler is all about this subject, so check out the article by clicking on the image above.

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Geology, Mount Rainier National Park, National Parks, National Parks Traveler

Red Spouter Is A Great Example Of Cool Geology

Red Spouter fumerole at Fountain Paint Pots, Yellowstone National Park during summer 2018
A close-up view of Red Spouter as a fumerole during summer 2018
Red Spouter as a hot spring (or really wet mud pot – take your pick) in the winter (February) of 2022

Geology is such a cool science. I have degrees in geology (which meant, at the time, diddly squat in terms of getting a job, but it was a cool branch of science to study, anyway). Yellowstone National Park is a great place to see geology, past and present. Take Red Spouter, for example.

Before August 1959, Red Spouter did not even exist. In its place was a small grassy hill in the Fountain Paint Pots area. Then, on August 17, 1959, the Hebgen Lake earthquake occurred about 25 miles northwest of Fountain Paint Pots with a magnitude of 7.3. It was quite a shaker and “rippled through Yellowstone,” creating Red Spouter.

The interesting thing about Red Spouter is, depending upon the season, it can be a hot spring, a mudpot, or a fumerole. Back in the summer of 2018, as I was moving from TX to central WA, I stopped for a brief visit to Yellowstone. At the time I explored the Fountain Paint Pots area, Red Spouter was a fumerole (steam vent). During my recent February 2022 visit, I toured the same area while on a snowcoach trip, and Red Spouter was a splashing, muddy red, hot spring (well, maybe you’d call it a mud pot, although it seemed really watery to me).

Why is this? Well, it all depends upon the water table just beneath the surface. If the water table is high, like when snow melts and in the spring, then it’s either a splashing hot spring or a bubbling mudpot. If the water table is low, which it can be during the height of a dry summer (and it’s pretty dry out in Yellowstone, anyway), then Red Spouter is a steam vent.

Geology is cool, and it’s even cooler when you can get nicely-composed photos of that geology, right?

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Geology, National Parks, Photography, Yellowstone National Park

Alien Crash Site? Or Just A Little Hot Spring At Upper Geyser Basin?

This is just a close shot of a very small hot spring (maybe 3 feet in diameter, including the melted ground around it) I saw while walking on the boardwalks at Upper Geyser Basin in Yellowstone National Park one freezing February morning. It was a pretty thing, all bright and distinct against the white snow, and it reminded me of a favorite old 1950’s sci fi movie I watch all the time on my iPad when traveling (I listen to movies while editing photos). Anybody ever seen “The Thing From Another World?” Not the one with Kurt Russell, but the 1951 black-and-white version? To me, that’s a classic. The timing and overlapping of the dialog, the whole black-and-white scenario. I love it. Oh, the special effects are laughable, but I still like it way better than the 1982 film. Maybe it’s an age thing, but to me, the old movies are classics and always will be.

Anyway, where is this going, you may ask? Well, in the 1951 version, at one point, the plane with the scientists and the Airforce personnel are flying over the alien’s frozen-over crash spot, and it looks exactly like this little hot spring’s configuration right here. As a matter of fact, when I spotted this thermal spring, it was the first thing that popped into my head.

So, sometimes, you may photograph the things you see because they remind you of something else, right?

Copyright Rebecca L. Latson, all rights reserved.

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Filed under Geology, National Parks, Photography, Yellowstone National Park